The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.

The Pyrenean Axial Zone is characterized by thick series of metasedimentary and orthogneissic materials derived from pre-Variscan rocks. These sequences were intruded by large bodies of Variscan granitoids, some exposed after the Alpine orogeny. In the Eastern Pyrenees, a number of quartz veins of k...

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Detalles Bibliográficos
Autores: Fonseca, H.A.M., Canals i Sabaté, Àngels, Cires, J., Casas Tuset, Josep Maria
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/97249
Acceso en línea:https://hdl.handle.net/2445/97249
Access Level:acceso abierto
Palabra clave:Quars
Creus, Cap de (Catalunya)
Quartz
Creus, Cape (Catalonia)
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repository_id_str
spelling The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.Fonseca, H.A.M.Canals i Sabaté, ÀngelsCires, J.Casas Tuset, Josep MariaQuarsCreus, Cap de (Catalunya)QuartzCreus, Cape (Catalonia)The Pyrenean Axial Zone is characterized by thick series of metasedimentary and orthogneissic materials derived from pre-Variscan rocks. These sequences were intruded by large bodies of Variscan granitoids, some exposed after the Alpine orogeny. In the Eastern Pyrenees, a number of quartz veins of kilometric length and metric to decametric width, are present. Although these veins are mostly hosted by Variscan and pre-Variscan rocks, in the utheastern limit of the Roc de Frausa Massif, large fault related quartz bodies rossc utting Mesozoic sedimentary rocks, have also been recognized Liesa, 1988). The Roses giant quartz vein constitutes a remarkable example of the seregional scale quartz veins. It is located at the south ernportion of the Cap de Creus Massif, extending for 2700 mand reaching widths up to 25m. Apparently, the vein continues towards the NW depicting a much longer structure.SEM - Sociedad Española de Mineralogía2015info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/97249Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a:MACLA. Revista de la Sociedad Española de Mineralogía, 2015, vol. 20, p. 49-50(c) Fonseca, H.A.M. et al., 2015info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/972492026-05-27T06:46:51Z
dc.title.none.fl_str_mv The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
title The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
spellingShingle The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
Fonseca, H.A.M.
Quars
Creus, Cap de (Catalunya)
Quartz
Creus, Cape (Catalonia)
title_short The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
title_full The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
title_fullStr The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
title_full_unstemmed The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
title_sort The Roses giant quartz vein (Cap de Creus, Eastern Pyrenees): Geology and fluid inclusion data.
dc.creator.none.fl_str_mv Fonseca, H.A.M.
Canals i Sabaté, Àngels
Cires, J.
Casas Tuset, Josep Maria
author Fonseca, H.A.M.
author_facet Fonseca, H.A.M.
Canals i Sabaté, Àngels
Cires, J.
Casas Tuset, Josep Maria
author_role author
author2 Canals i Sabaté, Àngels
Cires, J.
Casas Tuset, Josep Maria
author2_role author
author
author
dc.subject.none.fl_str_mv Quars
Creus, Cap de (Catalunya)
Quartz
Creus, Cape (Catalonia)
topic Quars
Creus, Cap de (Catalunya)
Quartz
Creus, Cape (Catalonia)
description The Pyrenean Axial Zone is characterized by thick series of metasedimentary and orthogneissic materials derived from pre-Variscan rocks. These sequences were intruded by large bodies of Variscan granitoids, some exposed after the Alpine orogeny. In the Eastern Pyrenees, a number of quartz veins of kilometric length and metric to decametric width, are present. Although these veins are mostly hosted by Variscan and pre-Variscan rocks, in the utheastern limit of the Roc de Frausa Massif, large fault related quartz bodies rossc utting Mesozoic sedimentary rocks, have also been recognized Liesa, 1988). The Roses giant quartz vein constitutes a remarkable example of the seregional scale quartz veins. It is located at the south ernportion of the Cap de Creus Massif, extending for 2700 mand reaching widths up to 25m. Apparently, the vein continues towards the NW depicting a much longer structure.
publishDate 2015
dc.date.none.fl_str_mv 2015
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/97249
url https://hdl.handle.net/2445/97249
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a:
MACLA. Revista de la Sociedad Española de Mineralogía, 2015, vol. 20, p. 49-50
dc.rights.none.fl_str_mv (c) Fonseca, H.A.M. et al., 2015
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) Fonseca, H.A.M. et al., 2015
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv SEM - Sociedad Española de Mineralogía
publisher.none.fl_str_mv SEM - Sociedad Española de Mineralogía
dc.source.none.fl_str_mv Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
reponame:Dipòsit Digital de la UB
instname:Universidad de Barcelona
instname_str Universidad de Barcelona
reponame_str Dipòsit Digital de la UB
collection Dipòsit Digital de la UB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,300724

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